Page 121 - Hydrocarbon Exploration and Production Second Edition
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108                                                          Reservoir Fluids


          large open pore system. However, since the Karst features are connected downdip
          to the waterleg, this is usually followed by rapid and substantial water breakthrough.
             A further important reaction is the replacement of the Ca 2+  ion in calcium
          carbonate by a magnesium ion. The latter is smaller, hence ‘space’ or porosity is
          created in the mineral lattice by the replacement. The resulting mineral is dolomite
          and the increase in effective porosity can be as high as 13%. The process can be
          expressed as
                             2CaCO 3 þ Mg 2þ  ! CaMgðCO 3 Þ þ Ca 2þ
                                                        2
             The magnesium ion is made available by migrating pore waters. If the process is
          continuous on a geologic time scale, more and more Mg 2+  is introduced to the
          system and the porosity reduces again. The rock has been over-dolomitised.
             Carbonate reservoirs are usually affected to varying degrees by diagenesis.
          However, the process of dissolution and replacement is not limited to carbonates.
          Feldspar, for instance, is another family of minerals prone to early alterations.
             During drilling and production operations, the chemical equilibrium in the
          reservoir pore system may be disturbed. This is particularly true if drilling mud or
          injection water enter the formation. The resulting reaction can lead to the preci-
          pitation of minerals around the borehole or in the reservoir, and may severely damage
          productivity. The compatibility of formation water with fluids introduced during
          drilling and production therefore has to be investigated at an early stage.



               6.2. Reservoir Fluids

               Introduction and Commercial Application: This section introduces the various types
          of hydrocarbons which are commonly exploited in oil and gas field developments.
          The initial distribution of the fluids in the reservoir must be described to be able to
          estimate the hydrocarbons initially in place (HCIIP) in the reservoir. The
          relationship between the subsurface volume of HCIIP and the equivalent surface
          volume is important in estimating the stock tank oil initially in place (STOIIP) and
          the gas initially in place (GIIP). The basic chemistry and physical properties of the
          fluid types are used to differentiate the behaviour of the fluids under producing
          conditions. For the petroleum and process engineers, a representative description of
          the reservoir fluid type is important to predict how the fluid properties will change
          with pressure and temperature and is essential for the correct design of the surface
          processing facilities. Looking further downstream, the chemical engineer would be
          concerned about the composition of the hydrocarbon fluids to determine the yields
          of various fractions which may be achieved.


          6.2.1. Hydrocarbon chemistry
          The fluids contained within petroleum accumulations are mixtures of organic
          compounds, which are mostly hydrocarbons (molecules composed of hydrogen and
          carbon atoms), but may also include sulphur, nitrogen, oxygen and metal compounds.
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